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Daniel Moraetis

Researcher at University of Sharjah

Publications -  50
Citations -  816

Daniel Moraetis is an academic researcher from University of Sharjah. The author has contributed to research in topics: Soil water & Semail Ophiolite. The author has an hindex of 14, co-authored 49 publications receiving 662 citations. Previous affiliations of Daniel Moraetis include Technical University of Crete & Sultan Qaboos University.

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Chemical and thermal modification of natural HEU-type zeolitic materials from Armenia, Georgia and Greece

TL;DR: In this article, three HEU-type zeolites from Armenia, Georgia and Greece formed from alteration of volcanic glass were treated with dilute KOH and subsequently either reacted with 6N HCl or heated at 700 °C.
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High-frequency monitoring for the identification of hydrological and bio-geochemical processes in a Mediterranean river basin

TL;DR: In this article, a telemetric high-frequency hydrologic and water quality monitoring network was deployed to obtain data for the characterization of the hydrology and bio-geochemical processes of a complex Mediterranean watershed of Koiliaris River, Crete, Greece.
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Olive mill wastewater irrigation of maize: Impacts on soil and groundwater

TL;DR: In this paper, the authors evaluated the environmental impact of using weathered olive mill wastewater (OMW) for 5 years to irrigate a maize field with weathered OMW and found that the maize field received 6 times more nitrogen, 50 times more potassium and 2 times less phosphorous than the recommended fertilization rates.
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Origin and mobility of hexavalent chromium in North-Eastern Attica, Greece

TL;DR: An integrated framework that is comprised of field surveys of groundwater, surface water and soils, laboratory process experiments and hydrologic and geochemical modeling is used to identify the origin (anthropogenic versus geogenic sources), fate and transport of hexavalent Cr in Tertiary and Quaternary deposits of Oropos plain in Greece.
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Characterization and mobility of geogenic chromium in soils and river bed sediments of Asopos basin.

TL;DR: Chromium distribution in Asopos river bed was influenced from the eroded products derived from extensive areas with ultramafic rocks the last 5Ma, and the mobility of chromium release is limited due to existing attenuation capacity controlled by ferric oxides coatings on the soil and sediments.